These NNE and ne faults become a long transform fault system and formed a boundary between the eastern margin of China Continental Plate and Philippine Sea Plate.
这些北北东向和北东向断层形成一条巨长的转换断层系列，也是中国大陆板块东缘与菲律宾洋块的一条边界。
The East China Sea Shelf Basin is a marginal sea basin located on Continental crust of China eastern margin.
东海陆架盆地是位于中国大陆东部边缘大陆地壳之上的边缘海盆地。
The marginal sea crust is another kind of oceanic crust, which was formed after the basalt magma engulfed and devoured the tattered continental margin crust.
边缘海洋壳是玄武岩浆侵入并吞蚀破碎的大陆边缘地壳后形成的不同于大洋壳的新型洋壳。
The plate activity is weaker in the passive continental margin of the northern South China Sea, which is favorable for forming the large-scale gas field and gas hydrate reservoirs.
南海北部被动大陆边缘是板块活动相对较弱的地区，业已证实是巨大天然气田形成的有利场所，同时也是水合物发育的有利地区。
In the light of the sedimentary tectono-geochemistry of they formed in shallow sea of continental margin.
硅质岩沉积大地构造地球化学表明硅质岩的沉积环境是大陆边缘的浅海。
The South China Sea is one of the largest marginal seas in the western Pacific region, with its northern margin being characterized by a passive continental margin.
南海是西太平洋地区最大的边缘海之一，其北部具有被动大陆边缘特征。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
根据基底性质分析，探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
The major disruption of Machaoying-Panhe defines the active continental margin of the north China plate and the south margin of the Epicontinental Sea in the Paleozoic period.
马超营一一潘河大断裂，界定了古生代时期华北板块活动大陆边缘陆架与陆缘表海的南部边沿。
The South China Sea is a huge marginal sea at East-Asian continental margin, and a tectonic region of the transitional crust type from continental to oceanic.
南海是东亚大陆边缘的巨型陆缘海，属大陆—大洋过渡型地壳构造区。
According to the isotopic dating, it was emplaced into the active continental margin in Permian, which was resulted from the eastward subduction of the Tethys sea.
结合同位素测年结果及其它地质事件，确定是在二叠纪侵位于活动陆缘，是区内古特提斯洋向东俯冲消减作用的产物。
The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.
南海北部陆缘下NW-SE方向流动的地幔流的存在使得伸展活动具有由北向南发育的机制。
The existence of NW-SE direction mantle flow under the continental crust in the north continental margin of South China Sea made the extension activities migrate from north to south.
南海北部陆缘下NW-SE方向流动的地幔流的存在使得伸展活动具有由北向南发育的机制。
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